Multi-proxy analysis of sediment core NBP20-02 KC72 from Cranton Bay, Amundsen Sea Embayment, West Antarctica

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Main Authors: Heberlein, Marianne G, Totten, Rebecca L., Fernández, Rodrigo, Hillenbrand, Claus-Dieter, Byrne, Colton C, Wellner, Julia S
Format: Dataset Open Access
Language:en
Published: PANGAEA 2026
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author Heberlein, Marianne G
Totten, Rebecca L.
Fernández, Rodrigo
Hillenbrand, Claus-Dieter
Byrne, Colton C
Wellner, Julia S
author_facet Heberlein, Marianne G
Totten, Rebecca L.
Fernández, Rodrigo
Hillenbrand, Claus-Dieter
Byrne, Colton C
Wellner, Julia S
collection Datos científicos de ciencias marinas y ambientales
contents This dataset includes the multi-proxy analysis of sediment core NBP20-02 KC72, collected from Cranton Bay, a small, biologically productive, and bathymetrically isolated embayment north of Pine Island Glacier in the Amundsen Sea, West Antarctica. The data are used to reconstruct past environmental and oceanographic changes in the bay since the Late Pleistocene and throughout the Holocene. Parameters include magnetic susceptibility, sediment grain size analysis, bulk sediment stable carbon isotopes, and Total Organic Carbon (TOC), as well as counts of diatom species.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_990498
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Multi-proxy analysis of sediment core NBP20-02 KC72 from Cranton Bay, Amundsen Sea Embayment, West Antarctica
Heberlein, Marianne G
Totten, Rebecca L.
Fernández, Rodrigo
Hillenbrand, Claus-Dieter
Byrne, Colton C
Wellner, Julia S
Antarctica; diatoms; grain size analysis; Stable carbon isotope (δ13C); Total organic carbon (TOC)
This dataset includes the multi-proxy analysis of sediment core NBP20-02 KC72, collected from Cranton Bay, a small, biologically productive, and bathymetrically isolated embayment north of Pine Island Glacier in the Amundsen Sea, West Antarctica. The data are used to reconstruct past environmental and oceanographic changes in the bay since the Late Pleistocene and throughout the Holocene. Parameters include magnetic susceptibility, sediment grain size analysis, bulk sediment stable carbon isotopes, and Total Organic Carbon (TOC), as well as counts of diatom species.
title Multi-proxy analysis of sediment core NBP20-02 KC72 from Cranton Bay, Amundsen Sea Embayment, West Antarctica
topic Antarctica; diatoms; grain size analysis; Stable carbon isotope (δ13C); Total organic carbon (TOC)
url https://doi.org/10.1594/PANGAEA.990498